摘要
阿尔泰山位于中国、蒙古和苏联的交界处,分布着较完整的垂直地带性土壤。有关阿尔泰山山地土壤的垂直分布规律,已有报道。本试验研究土壤中铁、锰的形态分布特征及垂直地带性,其结果有助于了解阿尔泰山山地土壤的发生发展过程,为合理开发利用阿尔泰山山地土壤资源的途径提供科学依据。
The characteristics of the form distribution of Fe and Mn in soils of Altai Mountains were studied by the fractionation method. The exchangeable Fe, weak acid soluble Fe, oxides bound Fe, and organic matter bound Fe changed increasingly and residual Fe decreasingly, with increasing elevation, following the order of calcic brown soil, castanozem, chernozem, dark brown forest soil, subalpine meadow soil and alpine meadow soil. The form characteristics of Fe in Altai Mountains soils can be divided into two types: dry type and moist type. The Mn form distribution in soils was more complicated than Fe in soils. It was affected by climate, vegetation etc. especially by microbes, the differences of the behavior between Fe and Mn in soils, factors affecting on it, and its genetic significance were discussed.
出处
《干旱区研究》
CSCD
北大核心
1991年第4期10-14,共5页
Arid Zone Research
关键词
土壤
铁
锰
形态
阿尔泰山
Soil, Fe, Mn, fractionation, vertical zonality.
